Note:This page contains AI-generated content for informational and entertainment purposes only. It may contain inaccuracies. Raw event data is from USGS and EMSC. All statistics, lists, and derived information are generated by this site. Full disclaimerFound an error?
Location:
Period:
27 May 2024 11:04:21 - 4 Jun 2024 19:54:44 (8 days 8 hours 50 minutes)
Volcanoes in 100km radius:
None
Earthquakes:
132
3 swarms found nearby.
2010
PS20100405.1(92.8km)
4 Apr
1 hours
5 earthquakes
2020
S20200817.1(15.9km)
17 Aug
3 days 20 hours
58 earthquakes
2024
6 Jul
9 days 5 hours
101 earthquakes
AI-generated article — for informational and entertainment purposes only. May contain inaccuracies. Full disclaimerFound an error?

Seismic Swarm S20240527.1: Analysis of Recent Activity in Baja California

Seismic swarm S20240527.1 was recorded in Baja California, Mexico, beginning at 11:04 on 27 May 2024 and concluding at 19:54 on 4 June 2024. The events occurred approximately 93 km south-southwest of Alberto Oviedo Mota. Over a period of 200 hours and 50 minutes, a total of 132 earthquakes were detected.

Analysis of the first 100 events reveals a sequence dominated by low-to-moderate magnitude tremors. Magnitudes ranged primarily between 1.3 and 4.2, with the largest event reaching 4.2 shortly after initiation. Depths were generally shallow, concentrated between 0 and 23 km, consistent with activity along upper crustal fault structures. The swarm exhibited an initial burst of activity on 27 May, including multiple events above magnitude 3.0, followed by sustained lower-magnitude occurrences through early June. Later phases showed occasional spikes, such as several magnitude 3.3–3.6 events on 28 and 29 May.

This swarm aligns with the broader tectonic framework of the region, situated near the boundary between the Pacific and North American plates. The area experiences ongoing transform faulting and extension associated with the Gulf of California rift system. Historical records since 2000 indicate only two prior swarms in the vicinity: one in 2010 and another in 2020. These episodes underscore the episodic nature of clustered seismicity in this part of Baja California, where fluid migration or stress transfer along faults can trigger sequences without a single dominant mainshock.

The provided data from SeismoSight classification highlight the swarm's contained duration and event count, offering insight into local fault behavior. No significant escalation beyond magnitude 4.2 was observed in the initial 100 events, suggesting a self-limiting process typical of swarm-type activity in transform-margin settings.

References

SeismoSight internal swarm classification S20240527.1 (2024).
Regional tectonic summaries from standard geological surveys of the Pacific-North American plate boundary.